地下水の流動経路における原位置の酸化還元緩衝能力の評価 : 特に硫酸還元緩衝能力について Evaluation of in situ sulfate reduction as redox buffer capacity in groundwater flow path
For safety assessment of geological isolation, it is important to evaluate in situ redox buffer capacity in high-permeability zone as groundwater flow path. This study evaluated in situ sulfate reduction as redox buffer capacity in the conglomerate bedding in Toki Lignite-bearing Formation, which occurs at the lowest part of sedimentary rocks overlying basement granite. The bedding plays an important role as the main groundwater flow path. The result showed that in situ redox buffer capacity in the conglomerate bedding has been identified on first nine months, whereas in the following period the redox buffer capacity has not been identified for about fifteen months. This will be caused by the bedding became inappropriate for microbial survival as the organic matter which is needful for microbial activity was consumed. Thus, there will be limited redox buffer capacity in groundwater flow path even in formation including organic matter-bearing layer.
- 日本水文科学会誌 = Journal of Japanese Association of Hydrological Sciences
日本水文科学会誌 = Journal of Japanese Association of Hydrological Sciences 37(1), 3-8, 2007-02-28
THE JAPANESE ASSOCIATION OF HYDOROLOGICAL SCIENCES